Element #75 was isolated in 1908 by the Japanese chemist Masataka Ogawa and named Nipponium. He inadequately assigned it as element #43 (Technetium). From the modern chemical viewpoint it has to be considered to be element 75. (note).

In 1925 the discovery of elements #43 (Medeleyev's Eka-Manganese) and #75 (Dvi-Manganese), the last missing elements on the main periodic table, was announced by Walter Noddack (1893-1960), Ida Eva Tacke (1896-1978, she married in 1926 Walter Noddack) and Otto Berg (1873-).

Platinum ores were known to contain elements #24-29, 44-47, and 76-79, while rare-earth minerals (columbite, gadolinite) contain elements #39-42 and 72-74. Noddack and Tacke at the Physico-Technical Testing Office in Berlin started in 1922 with their attempts to separate elements #43 and #75, first from Platinum ore, but since that was too costly, soon continued with the rare-earth minerals. The X-ray specialist Otto Berg at Werner-Siemens Laboratory did the identification. The team found weak X-ray spectral lines when electrons excited the elements. After three years research, element #75 was separated from gadolinite and named Rhenium (Latin for the River Rhine), after the Rheinland (Rhineland), the homeland of Ida Tacke (she was born in Lackhausen/Wesel).

Shortly afterwards they separated element #43 and named it Masurium after Noddack's homeland, the Masurian province. Therefore, some historians of chemistry consider that both names contain a large dosis of nationalism: the Rhine region and the Masurian swamps were during the First World War the most succesfull battle places for the German troops. Their discovery of Masurium was not confirmed (see Technetium). By working up 660 kg of molybdenite they were able in 1928 to extract 1 g of Rhenium.

About the same time, element #75 was also discovered, independently by the British investigators F.H. Loring and J.F.G. Druce in manganese sulphate, and by the Czechs Jaroslav Heyrovský (1890-1967) and V. Dolejsek. I found no further information on these claims.

Rhine

The Rhine (German: Rhein; Dutch: Rijn; French: Rhin; Romansh: Rain; Italian: Reno; Latin: Rhenus; West Frisian Ryn) is one of the longest and most important rivers in Europe, at 1,320 km (820 mi), with an average discharge of more than 2,000 m3/s (71,000 cu ft/s).

The name of the Rhine derives from Gaulish Renos, and ultimately from the Proto-Indo-European root *reie- ("to move, flow, run"), which is also the root of words like river and run. The Reno River in Italy shares the same etymology. The spelling with -h- seems to be borrowed from the Greek form of the name, Rhenos, seen also in rheos, stream, and rhein, to flow
(note).

The Rhineland (Rheinland in German) today is the general name for areas along the river Rhine between Bingen and the Dutch border. To the west the area stretches to the borders with Luxemburg, Belgium and the Netherlands; on the eastern side it only encompasses the towns and cities along the river. Except for the Saar this area more or less corresponds with the modern use of the term
(note).